1996 Articles
Slip complexity in a crustal plane model of an earthquake fault
We study numerically the behavior of a two-dimensional elastic plate (a crustal plane) that terminates along one of its edges at a fault boundary. Slip-weakening friction at the boundary, inertial dynamics in the bulk, and uniform slow loading via elastic coupling to a substrate combine to produce a complex, deterministically chaotic sequence of slipping events. We observe a power-law distribution of small events and an excess of large events. For the small events, the moments scale with rupture length in a manner that is consistent with seismological observations. For the large events, rupture occurs in the form of narrow propagating pulses.
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Files
- MShawL96.pdf application/pdf 519 KB Download File
Also Published In
- Title
- Physical Review Letters
- DOI
- https://doi.org/10.1103/PhysRevLett.77.972
More About This Work
- Academic Units
- Lamont-Doherty Earth Observatory
- Seismology, Geology, and Tectonophysics
- Published Here
- June 18, 2013